{
  "bulletins": [
    {
      "regions": [
        {
          "regionID": "DE-BY-12"
        },
        {
          "regionID": "DE-BY-20"
        },
        {
          "regionID": "DE-BY-11"
        },
        {
          "regionID": "DE-BY-30"
        }
      ],
      "validTime": {
        "startTime": "2022-01-23T23:00:00+00:00",
        "endTime": "2022-01-24T23:00:00+00:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "1800"
          },
          "customData": [],
          "mainValue": "moderate"
        },
        {
          "elevation": {
            "upperBound": "1800"
          },
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S",
              "SW",
              "W",
              "NW"
            ]
          },
          "problemType": "new_snow",
          "comment": null
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Avalanche danger is expected to recede further amid stable high-pressure front conditions."
      },
      "bulletinID": "RID1458RGR1",
      "publicationTime": "2022-01-23T17:00:00+00:00",
      "avalancheActivityHighlights": "Caution: Danger of falling!",
      "avalancheActivityComment": "The avalanche danger is moderate above 1800m; below that altitude it is low. The main danger stems from the new snow of the last few days which can be triggered even by a single skier. However, slab avalanches tend to stay small. Avalanches can trigger in very steep terrain in all aspects. Furthermore, older but partly still trigger-sensitive snowdrift accumulations persist in steep terrain adjacent to ridgelines and in wind-loaded gullies and bowls.  ",
      "snowpackStructureComment": "The fresh snow of recent days was deposited atop a melt-freeze encrusted, compact and largely stable old snowpack and at intermediate altitudes is widely blanketed by a thin ice crust or a melt-freeze crust. At higher altitude, in places trigger-sensitive interim layers are embedded in the uppermost layers of the snowpack, and the snow masses can glide over the encrusted surfaces. The sun moistens during the course of the day on sunny slopes. All in all, the snowpack depths are below average, at lower altitudes a solid snow base is lacking in many places."
    },
    {
      "regions": [
        {
          "regionID": "DE-BY-41"
        },
        {
          "regionID": "DE-BY-42"
        },
        {
          "regionID": "DE-BY-51"
        },
        {
          "regionID": "DE-BY-43"
        },
        {
          "regionID": "DE-BY-52"
        }
      ],
      "validTime": {
        "startTime": "2022-01-23T23:00:00+00:00",
        "endTime": "2022-01-24T23:00:00+00:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "moderate"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S",
              "SW",
              "W",
              "NW"
            ]
          },
          "problemType": "new_snow",
          "comment": null
        },
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S",
              "SW",
              "W",
              "NW"
            ]
          },
          "problemType": "gliding_snow",
          "comment": null
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Avalanche danger is expected to recede further amid stable high-pressure front conditions."
      },
      "bulletinID": "RID1458RGR2",
      "publicationTime": "2022-01-23T17:00:00+00:00",
      "avalancheActivityHighlights": "New fallen snow of recent days still prone to triggering.",
      "avalancheActivityComment": "Avalanche danger is moderate. The main problem stems from the new fallen snow of recent days which in places can be triggered as slab avalanches by a single person engaged in snow sports. This is possible on steep slopes in all aspects, in particular close to ridgelines, in gullies and bowls, forest aisles filled with wind-transported snow and below protuberances in the terrain. Avalanches can grow to medium size.\r\nIn addition, the glide snow activity increases, in particular on steep grassy slopes where glide cracks have opened.",
      "snowpackStructureComment": "The new fallen snow and snowdrifts of the last few days have bonded and settled considerably due to mild temperatures. Locally, they were deposited atop a smooth ice crust or atop an encrusted old snowpack surface on which it can start gliding. At higher altitudes, in places trigger-sensitive interim layers are embedded in partly large snowdrift accumulations which are blanketed and therefore difficult to recognize. At transitions to the ground the snowpack is frequently moist; gliding movements of the snow masses increase. This applies in particular where the snowpack moistens during the course of the day due to solar radiation."
    },
    {
      "regions": [
        {
          "regionID": "DE-BY-60"
        }
      ],
      "validTime": {
        "startTime": "2022-01-23T23:00:00+00:00",
        "endTime": "2022-01-24T23:00:00+00:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "2000"
          },
          "customData": [],
          "mainValue": "considerable"
        },
        {
          "elevation": {
            "upperBound": "2000"
          },
          "customData": [],
          "mainValue": "moderate"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S",
              "SW",
              "W",
              "NW"
            ]
          },
          "problemType": "new_snow",
          "comment": null
        },
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "SE",
              "S",
              "SW"
            ]
          },
          "problemType": "wet_snow",
          "comment": null
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Avalanche danger is expected to recede further amid stable high-pressure front conditions."
      },
      "bulletinID": "RID1458RGR3",
      "publicationTime": "2022-01-23T17:00:00+00:00",
      "avalancheActivityHighlights": "Avalanche situation critical, in particular at high altitude!",
      "avalancheActivityComment": "Avalanche danger above 2000 m is considerable; below that altitude it is moderate. The main problem stems from the new fallen snow of recent days which in places can be triggered as slab avalanches by a single person engaged in snow sports. This is possible on steep slopes in all aspects, in particular close to ridgelines, in gullies and bowls, forest aisles filled with wind-transported snow and below protuberances in the terrain. At high altitudes, avalanches that are triggered can grow to large size.In addition, spontaneously releasing moist loose snow avalanches and isolated slab avalanches can be expected on sun-exposed steep rocky slopes during the course of the day.",
      "snowpackStructureComment": "The new fallen snow of recent days has settled considerably due to mild temperatures. Trigger-sensitive intermediate layers in the snowpack that formed while precipitation paused and amid changing wind impacts are found in the new snowpack masses as well as in the blanketed snowdrift accumulations. In addition, the fresh snow and the encrusted old snowpack surface have not bonded sufficiently. Due to solar radiation the snowpack moistens superficially, forfeits its firmness and can start gliding over the encrusted old snowpack surface. "
    }
  ]
}